| dc.creator |
Sánchez Cela, Vicente |
|
| dc.creator |
Aparicio, Alfredo |
|
| dc.date |
2008-02-12T09:01:47Z |
|
| dc.date |
2008-02-12T09:01:47Z |
|
| dc.date |
1997 |
|
| dc.date.accessioned |
2017-01-31T01:00:06Z |
|
| dc.date.available |
2017-01-31T01:00:06Z |
|
| dc.identifier |
http://hdl.handle.net/10261/2920 |
|
| dc.identifier.uri |
http://dspace.mediu.edu.my:8181/xmlui/handle/10261/2920 |
|
| dc.description |
The peridotite and related rocks of southern Spain and Northern Morocco were formed through polyphase processes by sialic matter than, at different P-T conditions transformed sedimentary-epimetamorphic materials |
|
| dc.description |
Peer reviewed |
|
| dc.format |
537322 bytes |
|
| dc.format |
application/pdf |
|
| dc.language |
eng |
|
| dc.publisher |
Academia de Ciencias Exactas, Físicas, Químicas y Naturales de Zaragoza |
|
| dc.relation |
Revista Academia Ciencias Zaragoza |
|
| dc.relation |
52, ,197-210 |
|
| dc.rights |
openAccess |
|
| dc.subject |
ultramafic sedimentary materials |
|
| dc.title |
A model for the formation of ultramafic rocks in the crust:Peridotites of southern Spain and Northern Morocco |
|
| dc.type |
Artículo |
|